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The ocean absorbs about 1/3 of the anthropogenic CO2 released to the atmosphere. As more CO2 accumulates in the ocean, the oceanic pH decreases, leading to ocean acidification. In order to better understand the carbon cycle in the ocean and associated long-term pH variation, we estimate CO2 exchange flux at the sea surface in the Pacific Ocean with the empirical method proposed by Sugimoto et al. (2012) exploiting the publically available oceanic dataset. The oceanic CO2, the air-sea CO2 flux, and pH are successfully evaluated for the Pacific Ocean from 1985 through 2008. The pH and CO2 absorption relation is then argued along with climatological influences during the ENSO events.

Analysis of Ocean Acidification in the Pacific Ocean Based on the Data-driven Evaluation of the Air-sea Carbon Dioxide Flux